Fundamentals
of
diffraction
angles, coordination polyhedra, etc. reasonable? If yes, move to step
9.
If
no, go to step
7
using the next best solution.
9.
The model of the crystal structure is verified and completed by
computing phases for all available (conventional) structure amplitudes
using the current structural model (Eq. 2.105) and successive calculation
of Fourier (Eq. 2.133)
and/or difference Fourier maps (Eq. 2.135). Once
all atoms are located, the complete structure is refined using least squares
technique against all available diffraction data.
10. If no solution is found, step 2 should be repeated with different
parameters and
lists(s) of reflections in the starting sets. It may be
necessary to expand or reduce the list of reflections under consideration
by changing the cut-off value of
Emin
from a standard value of 1.2.
2.14.3
Structure solution from powder diffraction data
Solving the crystal structure using either heavy atom or direct techniques
does not always work in a straightforward fashion even when the well-
resolved and highly accurate diffraction data from a single crystal are
available. The complicating factor in powder diffraction is borne by the
intrinsic overlap of multiple Bragg peaks. The latter may become especially
severe when the unit cell volume and complexity of the structure increase.
Thus, there is a fundamental difference between the accuracy of structure
amplitudes obtained from single crystal and powder diffraction data. The
former are always resolved,
i.e. there is only one combination of indices,
hkl,
per Bragg peak, whereas in the latter some reflections may be fully or
partially overlapped. The intensities of individual reflections
hkl
may still be
recovered from powder diffraction data but their accuracy is critically
dependent on both the degree of the overlap and the quality of the pattern.
Obviously, the absolute overlapping of some reflections makes it impossible
to obtain the individual intensities regardless of the quality of data, and only
the combined total intensity is known
(e.g. reflections 431 and 051 in both the
cubic and tetragonal crystal systems).
As established above, individual intensities (or structure amplitudes) of
Bragg reflections are needed in order to solve the crystal structure using
direct or Patterson methods.
In
the first case, accurate normalized structure
amplitudes are required to generate phase angles and to evaluate their
probabilities. In the second case, accurate structure amplitudes result in the
higher accuracy and resolution on the Patterson map.
Thus, when reflections overlap to a degree when the individual intensities
can no longer be considered reliable, they may be dealt with using two
different approaches: